Island Climate Update 22 - July 2002

July

Monthly climate

ENSO & SST

Forecast validation

Three-month outlook

Feature article

Data sources

In this issue

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    Feature article

    Southern Oscillation Index (SOI) adopted from Bureau of Meteorology, Australia.
    Click to enlarge
    Sub Surface Temperature along the Equator for May 2002 (adapted from TOA/TRITON).
    Click to enlarge
    Sub Surface Temperature along the Equator for June 2002 (adapted from TOA/TRITON).
    Click to enlarge
    El Niño Update
    More progress towards the evolution of an El Niño in the last month
    Probabilities have increased to 85% for an El Niño event affecting the whole of the Southwest Pacific by September this year.
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    Forecast validation

    Forecast validation
    Forecast period: April to June 2002
    Rainfall was projected to be above average in the Western and Eastern Kiribati and Vanuatu, and average to above average in New Caledonia, Fiji, Niue and Pitcairn Island. Average to below average rainfall was expected for much of the region from the Solomon Islands east to the Marquesas including the Northern Cooks, and central French Polynesia.
    Average rainfall was forecast for other areas.
    Rainfall was as expected for many of the forecast areas. However, it was higher than forecast in Samoa and the Marquesas and Austral Islands.
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    ENSO & SST

    ENSO and Sea Surface Temperatures
    Equatorial Pacific Ocean up to +1.5°C warmer than average
    El Niño likely if conditions persist
    In the tropical central Pacific, a band of anomalously warm water (+1.5°C above average) extends from Western Kiribati towards the coast of South America. An area of the Pacific which is also very much warmer than average lies southeast of Pitcairn Island (+2.0°C above average).
    Generally, most of the Southwest Pacific is warmer than average ( +1.0 to 1.5°C).
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    July

    An overview of the present climate in the tropical South Pacific Islands, with an outlook for the coming months, to assist in dissemination of climate information in the Pacific region.
    Number 22 – 11 July 2002
    June’s Climate: The South Pacific Convergence Zone (SPCZ) extended east from the Solomon Islands toward Tuvalu. However, it was virtually non-existent further east in the Southwest Pacific. A large area of enhanced convection with areas of above average rainfall affected the region from the Solomon Islands west to Papua-New Guinea.
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    Monthly climate

    Enhanced convection over Papua New Guinea and the Solomon Islands
    Below average rainfall from Fiji to the Southern Cook Islands
    In June, the SPCZ extended east from the Solomon Islands toward Tuvalu, being displaced north of its mean position in that region. However, it was virtually non- existent further east in the Southwest Pacific.
    A large area of enhanced convection with areas of above average rainfall affected the region from the Solomon Islands west to Papua-New Guinea. In the north, the ITCZ was further south than usual, enhancing rainfall and cloudiness over parts of Kiribati.
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    Three-month outlook

    Rainfall outlook for July to September 2002
    Above average rainfall in equatorial latitudes from Nauru to Kiribati
    Average to above average rainfall for the Solomon Islands, Vanuatu and Tuvalu
    Average to below average rainfall in New Caledonia, Fiji, Samoa Tokelaus and Marquesas
    Mainly around average rainfall in other areas
    In the Western Pacific, the South Pacific Convergence Zone (SPCZ) extended east from Solomon Islands to Tuvalu and was virtually non-exsistent further east during June.
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    Data sources

    Sources of South Pacific rainfall data
    This bulletin is a multi-national project with important collaboration from the following Pacific nations:
    American Samoa
    Australia
    Cook Islands
    Fiji
    French Polynesia
    Kiribati
    New Caledonia
    New Zealand
    Niue
    Papua New Guinea
    Pitcairn Island
    Samoa
    Solomon Islands
    Tokelau
    Tonga
    Tuvalu
    Vanuatu
    Requests for Pacific island climate data should be directed to the Meteorological Services concerned.
    Acknowledgements
    This bulletin is made possible with financial support from the New Zealand Agency for International Development (NZAID), Wellington, New Zealand, wi